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Ephemeral ecological speciation and the latitudinal biodiversity gradient

机译:临时生态形态与纬度生物多样性梯度

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The richness of biodiversity in the tropics compared to high-latitude parts of the world forms one of the most globally conspicuous patterns in biology, and yet few hypotheses aim to explain this phenomenon in terms of explicit microevolutionary mechanisms of speciation and extinction. We link population genetic processes of selection and adaptation to speciation and extinction by way of their interaction with environmental factors to drive global scale macroecological patterns. High-latitude regions are both cradle and grave with respect to species diversification. In particular, we point to a conceptual equivalence of "environmental harshness" and "hard selection" as eco-evolutionary drivers of local adaptation and ecological speciation. By describing how ecological speciation likely occurs more readily at high latitudes, with such nascent species especially prone to extinction by fusion, we derive the ephemeral ecological speciation hypothesis as an integrative mechanistic explanation for latitudinal gradients in species turnover and the net accumulation of biodiversity.
机译:与世界上高纬度地区相比,热带地区生物多样性的丰富性是生物学上全球范围内最明显的模式之一,但很少有假说旨在通过明确的物种形成和灭绝的微观进化机制来解释这一现象。我们通过与环境因素的相互作用将选择和适应的种群遗传过程与物种形成和灭绝联系起来,以驱动全球规模的宏观生态格局。就物种多样化而言,高纬度地区既是摇篮,又是坟墓。特别是,我们指出“环境苛刻性”和“硬选择”在概念上是等同的,它们是局部适应和生态物种形成的生态进化驱动力。通过描述生态物种形成在高纬度地区更容易发生的情况,尤其是这种新生物种特别容易因融合而灭绝,我们得出了短暂的生态物种学说假设,作为对物种周转中纬度梯度和生物多样性净积累的综合机制解释。

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